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WSDI significantly increased at a few grids in the western Finland (Figure 8(d)), while increases in CSDI were mainly found in the northern Finland (Figure 8(e)).
Both TN90p and WSDI in the northern Finland were significantly associated with the EA pattern (Figures 9(e) and 9(f)).
The present study indicates that warm temperature extreme events (TXx, TNx, SU25, TX90p, TN90p, and WSDI) were mostly controlled by the EA and SCA patterns.
Caption: Figure 5: Spatial distribution maps of base values for (a) FD, (b) ID, (c) SU25, (d) WSDI, and (e) CSDI in Finland during 1961-2011.
WSDI results across the region recorded positive slopes, with the largest being in the central-southern mountain area (Figure 10(c)).
Significant upward trends were also recorded in warm-related extreme temperature indices (TN90p, TX90p, and WSDI), a cold extreme index (TNn) and growing season length (GSL) during the study period, while significant downward trends were identified in cold-related extreme temperature indices (TN10p, TX10p, and CSDI) and for the diurnal temperature range (DTR).
The black line represents the linear trends for (a) TN10p, (b) TX10p, (c) CSDI, (d) TNn, (e) TN90p, (f) TX90p, (g) WSDI, (h) TXx, (i) DTR, and (j) GSL.
The black line represents the linear trends for (a) TN90p, (b) TX90p, (c) WSDI, and (d) TXx.
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